<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-4074152641526693101</id><updated>2011-07-28T00:26:16.478-07:00</updated><title type='text'>ESSEA-FHSU Green Team</title><subtitle type='html'>Welcome to the temporary discussion area for FHSU's GSCI 676 - Apprenticeship in Geology</subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>14</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-6909378879009824208</id><published>2007-10-19T18:49:00.000-07:00</published><updated>2007-10-19T19:09:26.195-07:00</updated><title type='text'>ESSEA Final Project part 2 - CSA</title><content type='html'>&lt;span style="font-weight: bold;font-size:130%;" &gt;&lt;span style="font-style: italic;"&gt;Causal Chains&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;1. E &gt; A &gt; B&lt;/span&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;    A hurricane is often accompanied by a phenomenon known as a “storm surge.”&lt;span style=""&gt;  &lt;/span&gt;The winds of a &lt;span style=""&gt; &lt;/span&gt;hurricane tend to be most intense in the right-forward quadrant of the storm.&lt;span style=""&gt;  &lt;/span&gt;This is a result of adding together the speed and direction of the winds associated with the hurricanes:&lt;span style=""&gt;  &lt;/span&gt;the movement of the storm itself over the earth, and the spiraling-inward winds.&lt;span style=""&gt;  &lt;/span&gt;When these two motions are in the same direction, their wind speeds add together, reinforcing each other.&lt;span style=""&gt;  &lt;/span&gt;This combined wind can push a large amount of water onshore and cause extensive wind damage to structures and life along the coast.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;     When a hurricane is out in the open ocean, the ocean’s surface bulges upward a bit – a few feet – under the eye of the hurricane because of the lower atmospheric pressure within the eye of the storm.&lt;span style=""&gt;  &lt;/span&gt;This bulge increases in height as it comes into progressively shallower water much as any ocean wave gains height as it enters shallower water.&lt;span style=""&gt;  &lt;/span&gt;The storm surge is often the most damaging aspect of the hurricane, producing massive and sustained flooding over a wide area and impacting animal and plant life.&lt;/p&gt;                 &lt;p class="MsoNormal"&gt;&lt;span style=""&gt;&lt;table align="left" cellpadding="0" cellspacing="0"&gt;&lt;tbody&gt;&lt;tr&gt;&lt;td&gt;&lt;br /&gt;&lt;/td&gt;  &lt;/tr&gt; &lt;/tbody&gt;&lt;/table&gt;  &lt;/span&gt;&lt;!--[endif]--&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/_0wl6WI3fJDg/RxlhPTfPmCI/AAAAAAAAAXk/oEnK_Re2TcM/s1600-h/hurricane.jpg"&gt;&lt;img style="cursor: pointer;" src="http://4.bp.blogspot.com/_0wl6WI3fJDg/RxlhPTfPmCI/AAAAAAAAAXk/oEnK_Re2TcM/s320/hurricane.jpg" alt="" id="BLOGGER_PHOTO_ID_5123232966667900962" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;/p&gt; &lt;p class="MsoNormal"&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;  &lt;p&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;2.&lt;span style=""&gt;  &lt;/span&gt;E &gt; A &gt; E &gt; A &gt; . . .&lt;/span&gt;&lt;br /&gt;    Hurricanes transfer large amounts of energy, heat and moisture from the ocean into the atmosphere.&lt;b&gt;&lt;br /&gt;&lt;/b&gt;&lt;a href="http://www.sciencedaily.com/releases/2005/01/050110114115.htm"&gt;http://www.sciencedaily.com/releases/2005/01/050110114115.htm&lt;/a&gt;&lt;br /&gt;&lt;span style=""&gt;            &lt;/span&gt;    The temperature of a substance is a relative measure of the average kinetic energy of the particles within the substance.&lt;span style=""&gt;  &lt;/span&gt;Thus, water at 30&lt;sup&gt;o&lt;/sup&gt;C will have a normalized distribution of slow, average, and fast particles.&lt;span style=""&gt;  &lt;/span&gt;These faster particles can attain enough energy to escape the liquid state completely and evaporate.&lt;span style=""&gt;  &lt;/span&gt;Of course, as the temperature of the substance increases, more particles will gain enough energy to escape into the vapor stage.&lt;br /&gt;&lt;span style=""&gt;            &lt;/span&gt;     Normally, this evaporation – escape of higher-energy water particles – results in lowering the average kinetic energy of the particles left behind in the liquid state.&lt;span style=""&gt;  &lt;/span&gt;Hence, the phenomenon of evaporative cooling.&lt;span style=""&gt;  &lt;/span&gt;Effectively, the water vapor has carried some of the energy from the ocean into the atmosphere.&lt;br /&gt;&lt;span style=""&gt;            &lt;/span&gt;     As the mass of air containing this water vapor rises into the atmosphere, it undergoes expansion as it encounters the decreasing atmospheric pressure at higher altitudes.&lt;span style=""&gt;  &lt;/span&gt;As the air mass expands, it cools, and the water vapor condenses back into the liquid state.&lt;span style=""&gt;  &lt;/span&gt;Each kilogram of water that condenses releases 3.30 x 10&lt;sup&gt;5&lt;/sup&gt; J back into the atmosphere – almost 80 times the amount of energy required to change the temperature of that one kilogram of water by 1&lt;sup&gt;o&lt;/sup&gt;C.&lt;span style=""&gt;  &lt;/span&gt; This relatively massive amount of energy is released into the surrounding atmosphere and tends to add energy to the ocean surface below, resulting in increased evaporation rates..&lt;span style=""&gt;  &lt;/span&gt;This energy also causes increased wind speed, which encourages further evaporation from the surface by breaking the surface into smaller droplets.&lt;span style=""&gt;  &lt;/span&gt;Increased evaporation carries more energy into the atmosphere, releasing more energy as the latent heat of condensation.&lt;span style=""&gt;  &lt;/span&gt;The hurricane acts as a system in resonance with each event reinforcing the effects of the other events.&lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;3.&lt;span style=""&gt;  &lt;/span&gt;&lt;b style=""&gt;E &gt; H &gt; A&lt;/b&gt;&lt;/span&gt;&lt;b style=""&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt; text-indent: 0.5in;"&gt;When wind speeds increase, ocean turbulence increases, resulting in greater rates of evaporation from the ocean surface.&lt;span style=""&gt;  &lt;/span&gt;As wind speed increases, the amount of ocean spray increases; this spray is simply the ocean surface broken up into smaller volumes.&lt;span style=""&gt;  &lt;/span&gt;As the surface area of a given mass of water increases, it becomes more likely that water particles can escape the liquid state because they’re now nearer the surface of the water.&lt;span style=""&gt;  &lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt; text-indent: 0.5in;"&gt;For example, one cubic meter of water measures 1 m x 1 m x 1 m.&lt;span style=""&gt;  &lt;/span&gt;The surface of this cubic meter of water is 6 x (1 m x 1 m) = 6 m&lt;sup&gt;2&lt;/sup&gt; of surface area.&lt;span style=""&gt;  &lt;/span&gt;On the other hand, if this much water is broken up into cubic centimeters, there will be (100 cm x 100 cm x 100 cm) = 10&lt;sup&gt;6&lt;/sup&gt; cm&lt;sup&gt;3&lt;/sup&gt; of water.&lt;span style=""&gt;  &lt;/span&gt;The surface area for each of these tiny packages of water is 6 x (10&lt;sup&gt;-2&lt;/sup&gt; m x 10&lt;sup&gt;-2&lt;/sup&gt; m) = 6 x 10&lt;sup&gt;-4&lt;/sup&gt; m&lt;sup&gt;2&lt;/sup&gt;.&lt;span style=""&gt;  &lt;/span&gt;Multiply this surface area per cm&lt;sup&gt;3&lt;/sup&gt; by 10&lt;sup&gt;6&lt;/sup&gt; of these cubes, and there are 6 x 10&lt;sup&gt;2&lt;/sup&gt; m&lt;sup&gt;2&lt;/sup&gt; of surface area – 100 times as much surface area, and now the same number of water particles (remember, the mass of water didn’t change, it was just re-packaged) will be much closer to the surface and more likely to be evaporated.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt; text-indent: 0.5in;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/b&gt;&lt;/p&gt; &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;4.&lt;span style=""&gt;  &lt;/span&gt;E&gt;B&gt;A&gt;H&lt;/span&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;    &lt;p style="margin: 0in 0in 0.0001pt;"&gt;    High wind speeds produce large ocean waves, which in turn can damage the framework of coral reefs.&lt;span style=""&gt;  &lt;/span&gt;The amount of damage to massive corals is slight, but more delicate coral structures can face 99% damage.&lt;br /&gt;&lt;a href="http://www.int-res.com/articles/meps/78/m078p201.pdf"&gt;http://www.int-res.com/articles/meps/78/m078p201.pdf&lt;/a&gt; &lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;    Coral reefs act as large carbon sinks.&lt;span style=""&gt;  &lt;/span&gt;As coral reefs are destroyed, less carbon can be stored in the ocean and more is available to the atmosphere, resulting in increased concentrations of CO&lt;sub&gt;2&lt;/sub&gt; and increased atmospheric temperatures.&lt;span style=""&gt;  &lt;/span&gt;These increased atmospheric temperatures result in increased ocean temperatures, which may increase the intensity of hurricanes. &lt;/p&gt;   &lt;p class="MsoNormal"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;5. E &gt; B &gt; A&lt;/span&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;    53% of the &lt;st1:country-region&gt;&lt;st1:place&gt;US&lt;/st1:place&gt;&lt;/st1:country-region&gt; population and 55% of the world’s population lives within 50 miles of a coastline.&lt;span style=""&gt;  &lt;/span&gt;This increase in development and property values means that even if hurricanes do not change in frequency or intensity, we still face horrific costs with each successive hurricane.&lt;span style=""&gt;  &lt;/span&gt;Low-lying, developing countries such as &lt;st1:country-region&gt;&lt;st1:place&gt;Bangladesh&lt;/st1:place&gt;&lt;/st1:country-region&gt; and &lt;st1:country-region&gt;&lt;st1:place&gt;India&lt;/st1:place&gt;&lt;/st1:country-region&gt; face increased risk of large numbers of human fatalities if there’s an increase in hurricane frequency or intensity.&lt;span style=""&gt;  &lt;/span&gt;&lt;br /&gt;&lt;a href="http://www.noaanews.noaa.gov/stories2007/s2811.htm"&gt;http://www.noaanews.noaa.gov/stories2007/s2811.htm&lt;/a&gt; ; &lt;a href="http://www8.nos.noaa.gov/nccos/npe/projectdetail.aspx?id=61&amp;amp;fy=2007"&gt;http://www8.nos.noaa.gov/nccos/npe/projectdetail.aspx?id=61&amp;amp;fy=2007&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;     When nations must be concerned more about protecting their citizens from imminent and frequent flooding, they will be less concerned with regulating their carbon emissions.&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt; &lt;/span&gt;&lt;/p&gt;   &lt;p class="MsoNormal"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;6.&lt;span style=""&gt;  &lt;/span&gt;&lt;span style=""&gt;E &gt; B &gt; B&lt;/span&gt;&lt;/span&gt;&lt;span style=""&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;    A hurricane can strip coastal forests of branches and leaves, uproot trees with weak root systems, and the resulting leaf litter on the forest floor can choke out the undergrowth.&lt;span style=""&gt;  &lt;/span&gt;The torrential rainfall can produce mudslides which in turn devastate an area’s ecology.&lt;span style=""&gt;    &lt;/span&gt;Water left standing can contribute to increased mosquito populations and the accompanying malaria &amp;amp; dengue fever.&lt;br /&gt;&lt;a href="http://emissionhq.com/2weeks/hitsPuertoRico.aspx"&gt;http://emissionhq.com/2weeks/hitsPuertoRico.aspx&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;     DDT is still the insecticide of choice (National Geographic, August 2007) for eradicating malaria-bearing mosquitoes.&lt;span style=""&gt;  &lt;/span&gt;If nations use more DDT, the biosphere will undergo other changes in the quantity and quality of its waterfowl a la Rachel Carson’s “Silent Spring.” &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p class="MsoNormal"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;7. &lt;span style=""&gt;B &gt; E &gt; A &gt; H&lt;/span&gt;&lt;/span&gt;&lt;span style=""&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;    In the past, coastal wetlands have served as buffers between hurricanes and populated areas.&lt;span style=""&gt;  &lt;/span&gt;With the coastal wetlands disappearing at a rate (in &lt;/span&gt;&lt;st1:state&gt;&lt;st1:place&gt;&lt;span style=""&gt;Louisiana&lt;/span&gt;&lt;/st1:place&gt;&lt;/st1:state&gt;&lt;span style=""&gt;) of 25 square miles per year, populated areas will see more damage and fatalities from hurricanes even if the intensity and frequency of hurricanes does not increase.&lt;br /&gt;&lt;a href="http://www.washingtonpost.com/wp-dyn/content/article/2005/11/10/AR2005111000138_pf.html"&gt;http://www.washingtonpost.com/wp-dyn/content/article/2005/11/10/AR2005111000138_pf.html&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;&lt;span style=""&gt;            &lt;/span&gt;     Likewise, as wetlands are replaced with developments, an area loses its capability for carbon sequestration.&lt;span style=""&gt;  &lt;/span&gt;This lack can lead to increased concentrations of CO&lt;sub&gt;2&lt;/sub&gt; in the atmosphere, resulting in increased global temperatures in the atmosphere and then in the oceans.&lt;span style=""&gt;  &lt;/span&gt;These increased temperatures could help increase the intensity of hurricanes. &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p class="MsoNormal"&gt;&lt;b style=""&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;8. H &gt; L &gt; B&lt;/span&gt;&lt;/b&gt; &lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;    Rainfall causes increased water flow resulting in increased erosion.&lt;span style=""&gt;  &lt;/span&gt;In turn, this leads to greater sediment levels in the rivers which are deposited as the velocity of the water decreases downstream.&lt;span style=""&gt;  &lt;/span&gt;The good news is that this increased sediment load can help buoy up sinking river deltas.&lt;span style=""&gt; &lt;/span&gt;On the other hand, the &lt;st1:state&gt;&lt;st1:place&gt;Mississippi&lt;/st1:place&gt;&lt;/st1:state&gt;’s sediment load has decreased by 25% over the past several decades, and the &lt;st1:place&gt;Mississippi  River&lt;/st1:place&gt; delta – upon which the city of &lt;st1:city&gt;&lt;st1:place&gt;New   Orleans&lt;/st1:place&gt;&lt;/st1:city&gt; is located – is sinking as a result.&lt;span style=""&gt;  &lt;/span&gt;This in turn leads to the potential for more damage from the storm surges that accompany hurricanes. &lt;/p&gt;   &lt;p class="MsoNormal"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;      &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;9.&lt;span style=""&gt;  &lt;/span&gt;L &gt; A &gt; L &gt; A .&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; &lt;/span&gt;&lt;/b&gt;&lt;span style="color:yellow;"&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;. .&lt;/span&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;br /&gt;    Eroded, barren land can give up more dust into the atmosphere, providing more condensation nuclei for water vapor.&lt;span style=""&gt;  &lt;/span&gt;Greater precipitation over these areas will result in even more erosion, exacerbating the problem.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/b&gt;&lt;/p&gt; &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;br /&gt;10. H &gt; A &gt; H &gt; A . . .&lt;/span&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;    &lt;p style="margin: 0in 0in 0.0001pt;"&gt;    The warm ocean water provides water vapor to the atmosphere, and its condensation provides energy for further evaporation of water from the ocean surface.&lt;span style=""&gt;  &lt;/span&gt;This feedback loop, aided by lack of wind shear in the upper atmosphere, provides the impetus for hurricane formation and intensification. &lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-6909378879009824208?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/6909378879009824208/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=6909378879009824208&amp;isPopup=true' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6909378879009824208'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6909378879009824208'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/10/essea-final-project-part-2-csa.html' title='ESSEA Final Project part 2 - CSA'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_0wl6WI3fJDg/RxlhPTfPmCI/AAAAAAAAAXk/oEnK_Re2TcM/s72-c/hurricane.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-4142664377331069708</id><published>2007-10-19T18:45:00.000-07:00</published><updated>2007-10-19T18:48:43.720-07:00</updated><title type='text'>ESSEA Final Project Part I- CSA</title><content type='html'>&lt;span style="font-size:130%;"&gt;&lt;span style="font-style: italic;"&gt;Event-Sphere and Sphere-Sphere Interactions&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;  &lt;p&gt;&lt;b&gt;Event and Atmosphere:&lt;span style=""&gt;  &lt;/span&gt;Hurricane&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p&gt;&lt;b&gt;E &gt; A&lt;br /&gt;&lt;/b&gt;Hurricanes transfer large amounts of energy, heat and moisture from the ocean into the atmosphere.&lt;b&gt;&lt;br /&gt;&lt;/b&gt;&lt;a href="http://www.sciencedaily.com/releases/2005/01/050110114115.htm"&gt;http://www.sciencedaily.com/releases/2005/01/050110114115.htm&lt;/a&gt;&lt;br /&gt;&lt;span style=""&gt;            &lt;/span&gt;Energy is needed to change water from a liquid to vapor, and as water evaporates it transfers energy from the ocean to the atmosphere.&lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; A&lt;br /&gt;&lt;/b&gt;Hurricanes produce large variations in atmospheric pressure across the radius of the storm, with the lowest pressure present in the central ‘eye’ of the storm.&lt;span style=""&gt;  &lt;/span&gt;Hurricane strength is measured in terms of maximum sustained wind speed and the barometric pressure within the eye.&lt;span style=""&gt;  &lt;/span&gt;Lower barometric pressures result in greater wind speeds because the wind is a result of the air moving from a region of higher pressure to a region of lower pressure.&lt;span style=""&gt;  &lt;/span&gt;As the pressure gradient increases, so does the wind speed.&lt;span style=""&gt;  &lt;/span&gt;This phenomena can be compared to siphoning gas from a car tank:&lt;span style=""&gt;  &lt;/span&gt;as the mouth-sucking end of the hose is lowered, the gas comes out faster.&lt;span style=""&gt;  &lt;/span&gt;The Coriolis effect then causes the familiar spiral formation as the inward-rushing winds are acted upon by the earth’s rotation.&lt;span style=""&gt;  &lt;/span&gt;Contrary to popular opinion, the Coriolis effect is not the factor influencing short-term phenomena such as water swirling down a drain.&lt;span style=""&gt;  &lt;/span&gt;The Coriolis forces act over a large area over a relatively long time.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;A &gt; E&lt;br /&gt;&lt;/b&gt;Presence of high wind shear in the upper atmosphere prevents hurricanes from forming.&lt;br /&gt;&lt;a href="http://environment.newscientist.com/channel/earth/hurricane-season/dn11633-wind-shear-may-cancel-climates-effect-on-hurricanes.html"&gt;http://environment.newscientist.com/channel/earth/hurricane-season/dn11633-wind-shear-may-cancel-climates-effect-on-hurricanes.html&lt;/a&gt; &lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;            &lt;/span&gt;In order for the cycle of evaporation-rising altitude-condensation-release of energy to occur, lateral wind currents at the upper atmosphere must be minimal.&lt;span style=""&gt;  &lt;/span&gt;This is because wind shear would cause the energy to dissipate and disrupt the flow of winds rushing in to the center of low pressure at the eye of the storm.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;A &gt; E&lt;/b&gt;&lt;br /&gt;Hurricanes form when energy is released into the atmosphere from the condensation of water vapor in the upper atmosphere.&lt;span style=""&gt;  &lt;/span&gt;It seems to follow that increased ocean temperatures will promote increased evaporation of water from the ocean into the atmosphere, providing a greater amount of energy that could be used to form or intensify hurricanes.&lt;br /&gt;&lt;a href="http://www.physicstoday.org/vol-59/iss-8/p74.html"&gt;http://www.physicstoday.org/vol-59/iss-8/p74.html&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;Event and Hydrosphere:&lt;span style=""&gt;  &lt;/span&gt;Hurricane&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; H&lt;br /&gt;&lt;/b&gt;As hurricanes pass over open warm water, energy is released from the water into the hurricane leaving a region of much cooler water in the storm’s wake.&lt;span style=""&gt;  &lt;/span&gt;This follows the law of conservation of energy – that energy entering one part of a closed system had as its source another part of the closed system.&lt;span style=""&gt;  &lt;/span&gt;True, the earth isn’t a closed system, but the regions of water surface/overlying air could be considered as such over a fairly large area.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;H &gt; E&lt;br /&gt;&lt;/b&gt;Increased ocean temperatures lead to increased rates of surface evaporation, which in turns provides more energy to fuel the hurricane’s development.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;Event and Biosphere: Hurricane&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; B&lt;br /&gt;&lt;/b&gt;Hurricanes stir up the ocean, resulting in phytoplankton blooms forming in their wake.&lt;br /&gt;&lt;a href="http://www.nasa.gov/centers/goddard/news/topstory/2004/0602hurricanebloom.html"&gt;http://www.nasa.gov/centers/goddard/news/topstory/2004/0602hurricanebloom.html&lt;/a&gt; &lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;            &lt;/span&gt;As hurricanes stir up the oceans over which they pass, nutrients are brought up from the depths.&lt;span style=""&gt;  &lt;/span&gt;Phytoplankton which depend on these nutrients can now access them in the zones of light upon which they’re dependent, resulting in increased populations of phytoplankton.&lt;span style=""&gt;  &lt;/span&gt;The magnitude of these blooms depends on the size, strength, and duration of the hurricanes.&lt;br /&gt; &lt;!--[if !supportLineBreakNewLine]--&gt;&lt;br /&gt; &lt;!--[endif]--&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; B&lt;br /&gt;&lt;/b&gt;High wind speeds produce large ocean waves, which in turn can damage the framework of coral reefs.&lt;span style=""&gt;  &lt;/span&gt;The amount of damage to massive corals is slight, but more delicate coral structures can face 99% damage.&lt;br /&gt;&lt;a href="http://www.int-res.com/articles/meps/78/m078p201.pdf"&gt;http://www.int-res.com/articles/meps/78/m078p201.pdf&lt;/a&gt; &lt;br /&gt; &lt;!--[if !supportLineBreakNewLine]--&gt;&lt;br /&gt; &lt;!--[endif]--&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; B&lt;br /&gt;&lt;/b&gt;53% of the &lt;st1:country-region&gt;&lt;st1:place&gt;US&lt;/st1:place&gt;&lt;/st1:country-region&gt; population and 55% of the world’s population lives within 50 miles of a coastline.&lt;span style=""&gt;  &lt;/span&gt;This increase in development and property values means that even if hurricanes do not change in frequency or intensity, we still face horrific costs with each successive hurricane.&lt;span style=""&gt;  &lt;/span&gt;Low-lying, developing countries such as &lt;st1:country-region&gt;&lt;st1:place&gt;Bangladesh&lt;/st1:place&gt;&lt;/st1:country-region&gt; and &lt;st1:country-region&gt;&lt;st1:place&gt;India&lt;/st1:place&gt;&lt;/st1:country-region&gt; face increased risk of large numbers of human fatalities if there’s an increase in hurricane frequency or intensity.&lt;span style=""&gt;  &lt;/span&gt;&lt;br /&gt;&lt;a href="http://www.noaanews.noaa.gov/stories2007/s2811.htm"&gt;http://www.noaanews.noaa.gov/stories2007/s2811.htm&lt;/a&gt; ; &lt;a href="http://www8.nos.noaa.gov/nccos/npe/projectdetail.aspx?id=61&amp;amp;fy=2007"&gt;http://www8.nos.noaa.gov/nccos/npe/projectdetail.aspx?id=61&amp;amp;fy=2007&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; B&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;A hurricane can strip coastal forests of branches and leaves, uproot trees with weak root systems, and the resulting leaf litter on the forest floor can choke out the undergrowth.&lt;span style=""&gt;  &lt;/span&gt;The torrential rainfall can produce mudslides which in turn devastate an area’s ecology.&lt;span style=""&gt;    &lt;/span&gt;Water left standing can contribute to increased mosquito populations and the accompanying malaria &amp;amp; dengue fever.&lt;br /&gt;&lt;a href="http://emissionhq.com/2weeks/hitsPuertoRico.aspx"&gt;http://emissionhq.com/2weeks/hitsPuertoRico.aspx&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;B &gt; E&lt;br /&gt;&lt;/b&gt;&lt;span style=""&gt;In the past, coastal wetlands have served as buffers between hurricanes and populated areas.&lt;span style=""&gt;  &lt;/span&gt;With the coastal wetlands disappearing at a rate (in &lt;/span&gt;&lt;st1:state&gt;&lt;st1:place&gt;&lt;span style=""&gt;Louisiana&lt;/span&gt;&lt;/st1:place&gt;&lt;/st1:State&gt;&lt;span style=""&gt;) of 25 square miles per year, populated areas will see more damage and fatalities from hurricanes even if the intensity and frequency of hurricanes does not increase.&lt;br /&gt;&lt;a href="http://www.washingtonpost.com/wp-dyn/content/article/2005/11/10/AR2005111000138_pf.html"&gt;http://www.washingtonpost.com/wp-dyn/content/article/2005/11/10/AR2005111000138_pf.html&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;&lt;span style=""&gt;            &lt;/span&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;Event and Lithosphere: Hurricane&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;E &gt; L&lt;br /&gt;&lt;/b&gt;Extreme amounts of rainfall can result in mudslides and substantial erosion of beaches and coastal plains.&lt;span style=""&gt;  &lt;/span&gt;Rivers can carve new channels due to their increased discharge.&lt;br /&gt;&lt;a href="http://emissionhq.com/2weeks/hitsPuertoRico.aspx"&gt;http://emissionhq.com/2weeks/hitsPuertoRico.aspx&lt;/a&gt; &lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b&gt;&lt;br /&gt;&lt;/b&gt;.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;Sphere-Sphere Interactions: Hurricane&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;Lithosphere&lt;/b&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial; font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;=&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt; &lt;/span&gt;&lt;/b&gt;&lt;b style=""&gt;&lt;span style="font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;/span&gt;&lt;/span&gt;Hydrosphere&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;Rainfall causes increased water flow resulting in increased erosion.&lt;span style=""&gt;  &lt;/span&gt;In turn, this leads to greater sediment levels in the rivers which is deposited as the velocity of the water decreases downstream.&lt;span style=""&gt;  &lt;/span&gt;The good news is that this increased sediment load can help buoy up sinking river deltas.&lt;span style=""&gt;  &lt;/span&gt;For example, the &lt;st1:state&gt;&lt;st1:place&gt;Mississippi&lt;/st1:place&gt;&lt;/st1:State&gt;’s sediment load has decreased by 25% over the past several decades, and the &lt;st1:place&gt;Mississippi  River&lt;/st1:place&gt; delta – upon which the city of &lt;st1:city&gt;&lt;st1:place&gt;New   Orleans&lt;/st1:place&gt;&lt;/st1:City&gt; is located – is sinking as a result.&lt;span style=""&gt;  &lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;Lithosphere &lt;/b&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial; font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;=&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;/span&gt;&lt;/b&gt;&lt;b style=""&gt;&lt;span style="font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;/span&gt;&lt;/span&gt; Biosphere&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;Eroded land and missing topsoil is less likely to support plant life, resulting in more erosion because there are no roots to keep the soil in place.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;Lithosphere &lt;/b&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial; font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;=&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;/span&gt;&lt;/b&gt;&lt;b style=""&gt;&lt;span style="font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;/span&gt;&lt;/span&gt; Atmosphere&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;Eroded, barren land can give up more dust into the atmosphere, providing more condensation nuclei for water vapor.&lt;span style=""&gt;  &lt;/span&gt;The mere presence of water vapor at the right temperature and pressure is not enough for condensation to occur; the vapor needs a tiny bit of matter to cling to such as dust or smoke particles or sea salt from ocean spray. Hence, cloud seeding is used to “kick-start” rainfall in some areas.&lt;span style=""&gt;   &lt;/span&gt;The effect is analogous to “bubbles in a glass of beer.” &lt;span style=""&gt; &lt;/span&gt;Sure, a good, fresh beer is nice and frothy because the bubbles are speeding to the surface . . . but try adding some salt!&lt;span style=""&gt;  &lt;/span&gt;Yes, it ruins the taste, but just watch the froth magnify because the gas that’s dissolved in the liquid now has something to congregate around (nuclei), and the bubbles grow as they rise to the surface because more and more gas microbubbles are attracted to the larger bubble.&lt;span style=""&gt;  &lt;/span&gt;I’d thought this growth was explained by the decreased pressure within the liquid as the depth below the surface decreased; if you do the math, though (was it Stokes theorem?&lt;span style=""&gt;  &lt;/span&gt;Sorry, it’s been awhile, don’t remember the details), that factor doesn’t begin to account for the growth of the bubbles.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;span style=""&gt;            &lt;/span&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;Hydrosphere &lt;/b&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial; font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;=&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;/span&gt;&lt;/b&gt;&lt;b style=""&gt;&lt;span style="font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;/span&gt;&lt;/span&gt; Biosphere&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;Changes in water reservoirs lead to changes in the life in and surrounding them.&lt;span style=""&gt;  &lt;/span&gt;As water evaporates, the sediment load increases proportionately and fish species preferring clear water die out, leaving traditional bottom-feeders such as catfish, carp and gar.&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;Hydrosphere &lt;/span&gt;&lt;/b&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial; font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;=&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt; Atmosphere&lt;/span&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;/b&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;This is probably the most significant sphere-sphere interaction in the hurricane.&lt;span style=""&gt;  &lt;/span&gt;The warm ocean water provides water vapor to the atmosphere, and its condensation provides energy for further evaporation of water from the ocean surface.&lt;span style=""&gt;  &lt;/span&gt;This feedback loop, aided by lack of wind shear in the upper atmosphere, provides the impetus for hurricane formation and intensification. H &gt; A &gt; H &gt; A . . .&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;/p&gt;   &lt;p style="margin: 0in 0in 0.0001pt;"&gt;&lt;b style=""&gt;Biosphere &lt;/b&gt;&lt;b style=""&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial; font-family: Wingdings;"&gt;&lt;span style=""&gt;&lt;=&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="background: yellow none repeat scroll 0% 50%; -moz-background-clip: initial; -moz-background-origin: initial; -moz-background-inline-policy: initial;"&gt;&lt;/span&gt;&lt;/b&gt;&lt;b style=""&gt; Atmosphere&lt;/b&gt;&lt;br /&gt;??&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-4142664377331069708?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/4142664377331069708/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=4142664377331069708&amp;isPopup=true' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/4142664377331069708'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/4142664377331069708'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/10/essea-final-project-part-i-csa.html' title='ESSEA Final Project Part I- CSA'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-6311801365487378478</id><published>2007-09-21T04:11:00.000-07:00</published><updated>2007-09-21T04:12:44.351-07:00</updated><title type='text'>Questions from JoanS</title><content type='html'>I also want to learn how scientists collect their data, meaning, and processes involved.&lt;br /&gt;&lt;br /&gt;More questions&lt;br /&gt;&lt;br /&gt;Why is global warming a problem? If it is? How much warmer will the earth become? Effects of global warming?&lt;br /&gt;&lt;br /&gt;What can we do about global warming?&lt;br /&gt;&lt;br /&gt;With rising sea level, how much and how fast, and what are the effects? Will my favorite Hawaiian Islands disappear?&lt;br /&gt;&lt;br /&gt;Instead of global warming, I read the term climate - what about the changing climates? What will happen to western Kansas - if it has consecutive dry years again? Are the extreme and unusual weather events caused by global warming? or are they even extreme and unusual?&lt;br /&gt;&lt;br /&gt;One site asked? If Earth has warmed and cooled throughout history, what makes scientists think that humans are causing global warming now? I thought this also.&lt;br /&gt;&lt;br /&gt;I am fascinated with the increasing sea levels, why global warming a problem and the effects, and what we can do?&lt;br /&gt;&lt;br /&gt;There is so much info!!!! - JoanS&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-6311801365487378478?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/6311801365487378478/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=6311801365487378478&amp;isPopup=true' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6311801365487378478'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6311801365487378478'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/questions-from-joans.html' title='Questions from JoanS'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-9202662359995345851</id><published>2007-09-20T17:09:00.000-07:00</published><updated>2007-09-20T17:18:33.661-07:00</updated><title type='text'>Don't Panic!!!</title><content type='html'>&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://www.equinox-communications.com/shoppy/images/uploads/stress_head.gif"&gt;&lt;img style="margin: 0pt 0pt 10px 10px; float: right; cursor: pointer; width: 200px;" src="http://www.equinox-communications.com/shoppy/images/uploads/stress_head.gif" alt="" border="0" /&gt;&lt;/a&gt;I just took a look at our "real" class website, and lookie what I found:&lt;br /&gt;&lt;br /&gt;&lt;b&gt;Team Assignment&lt;/b&gt;&lt;b&gt;&lt;br /&gt;Team:&lt;/b&gt;  &lt;ul&gt; &lt;li&gt;Post your questions in the discussion space in the Teacher as Researcher Discussion Space.&lt;/li&gt;&lt;li&gt;Review your teammates' questions. &lt;/li&gt;&lt;li&gt;List the key questions and plan how to investigate them as a team.&lt;/li&gt;&lt;li&gt;List answers to your questions as you build knowledge together.&lt;/li&gt; &lt;/ul&gt; &lt;span style="color: rgb(255, 0, 0); font-weight: bold;"&gt;Deadline:  Monday, September 24 2007 11:59 PM (Central Time)&lt;/span&gt;&lt;br /&gt;&lt;br /&gt; Whew. &lt;br /&gt;&lt;br /&gt; . . . erm, I mean, uh, I have every confidence we could have finished the task tomorrow - we're getting some good collaboration going.  (Wheee!!!)&lt;br /&gt;&lt;br /&gt;But just think how much &lt;span style="font-style: italic;"&gt;better&lt;/span&gt; it'll be after we've had some time to cogitate over the weekend.  I don't know about y'all, but my brain needs time to muddle through ideas before there's any hope of coherent output.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-9202662359995345851?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/9202662359995345851/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=9202662359995345851&amp;isPopup=true' title='2 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/9202662359995345851'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/9202662359995345851'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/dont-panic.html' title='Don&apos;t Panic!!!'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>2</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-7646201167621311162</id><published>2007-09-20T15:03:00.001-07:00</published><updated>2007-09-20T17:41:59.382-07:00</updated><title type='text'>Some Global Warming Questions</title><content type='html'>&lt;a href="http://3.bp.blogspot.com/_yYGCT5WC4X0/RvLwra7diKI/AAAAAAAAABU/IUW60nFIr4Q/s1600-h/global_warming.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5112413155772696738" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; CURSOR: hand" alt="" src="http://3.bp.blogspot.com/_yYGCT5WC4X0/RvLwra7diKI/AAAAAAAAABU/IUW60nFIr4Q/s320/global_warming.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;Hey, all. I read Jana's questions in comments on one of the posts. Good questions, Jana! I have some of the same questions, and here are some additional questions for consideration:&lt;br /&gt;&lt;br /&gt;1) Can the noted changes in our earth system be explained by natural variability (including the observed changes in solar output)?&lt;br /&gt;2) How important and reliable are paleoclimatic trends in predicting the future when it comes to global warming or cooling?&lt;br /&gt;3) How reliable is the IPCC Special Report on Emission Scenarios in determining the range of future possible greenhouse gas concentrations?&lt;br /&gt;4) What factors do the IPCC and other trusted sources use to calculate these scenarios?&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-7646201167621311162?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/7646201167621311162/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=7646201167621311162&amp;isPopup=true' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/7646201167621311162'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/7646201167621311162'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/some-global-warming-questions.html' title='Some Global Warming Questions'/><author><name>Jenny</name><uri>http://www.blogger.com/profile/03981184493261191479</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='28' src='http://photos1.blogger.com/blogger/560/1369/1600/Jenny%201.JPG'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_yYGCT5WC4X0/RvLwra7diKI/AAAAAAAAABU/IUW60nFIr4Q/s72-c/global_warming.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-6918559100572405875</id><published>2007-09-19T17:29:00.000-07:00</published><updated>2007-09-19T17:37:00.674-07:00</updated><title type='text'>Cycle A - Teacher as Researcher - JS</title><content type='html'>&lt;p class="MsoNormal"&gt;&lt;span style=""&gt;            &lt;/span&gt;I agree and believe that humans have increased the amount of carbon dioxide in the atmosphere by the burning of fossil fuels, deforestation, and changing land use. The rapid increase in atmospheric concentrations of the three main human-made greenhouse gases&lt;span style=""&gt;  &lt;/span&gt;- carbon dioxide, methane, and nitrous oxide – is clear from the data sets for these gases over the last 420,000 years. &lt;span style=""&gt; &lt;/span&gt;&lt;a href="http://www.eoearth.org/"&gt;http://www.eoearth.org/&lt;/a&gt; &lt;span style=""&gt; &lt;/span&gt;&lt;span style="color:red;"&gt;How do scientists know this?&lt;/span&gt; Most of us own automobiles; run our heaters and air conditioners, clothes driers, dish washers, etc…most of us contribute to the greenhouse effect. Also look at industries today, traffic, amount of cars owned per family, number of homes, the earth’s infrastructure, and the means to achieve all this (deforestation and destruction of grasslands and vegetation. &lt;span style=""&gt; &lt;/span&gt;Deforestation is occurring - as I saw logging in &lt;st1:place&gt;Northwest North America&lt;/st1:place&gt; this summer from the airplane.&lt;span style=""&gt;  &lt;/span&gt;Deforestation (changes the amount of carbon dioxide consumed or absorbed by earth’s surface); hence, deforestation brings about other effects such as land erosion, contamination, upheaval of wildlife, drought, etc….&lt;span style=""&gt; &lt;/span&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;/p&gt; &lt;p class="MsoNormal"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;span style=""&gt;          &lt;/span&gt;&lt;br /&gt;It was noted that increases in the atmospheric concentration of carbon dioxide and other greenhouse gases strengthens the greenhouse effect &lt;a href="http://www.exploratorium.edu/climate/index.html"&gt;http://www.exploratorium.edu/climate/index.html&lt;/a&gt; and may contribute to global warming. Greenhouse effect meaning the sun heats the Earth and some of this heat, rather than escaping back to space, is trapped in the atmosphere by clouds and greenhouse gases, such as water vapor and carbon dioxide. The Green house effect is what makes Earth habitable. &lt;a href="http://serc.carleton.edu/introgeo/earthsytem/nutshell/index2.html"&gt;http://serc.carleton.edu/introgeo/earthsytem/nutshell/index2.html&lt;/a&gt; &lt;/p&gt;     &lt;p class="MsoNormal"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;span style="color:red;"&gt;&lt;span style=""&gt;           &lt;/span&gt;&lt;br /&gt;What gases (carbon dioxide, methane, nitrous oxide) cause the greatest significance to the greenhouse effect?&lt;span style=""&gt;  &lt;/span&gt;We are taking small steps to reduce the greenhouse effect (building green, recycling, conserving, but enough? What about developing countries that now want their share of energy and Americans that want to improve their standard of living? Will this intensify the greenhouse effect at an even greater accelerated rate? &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;   &lt;p&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;span style=""&gt;           &lt;/span&gt;&lt;br /&gt;It has been noted that global warming has contributed to more frequent and violent hurricanes. Recent studies have linked rising sea surface temperatures, or SSTs, in the &lt;st1:place&gt;Atlantic  Ocean&lt;/st1:place&gt; to climate change caused by human activities. Warmer SST's means the ocean is capable of storing more energy--energy that is converted to wind power during tropical storms. &lt;a href="http://www.livescience.com/environment/060815_gw_hurricanes.html"&gt;http://www.livescience.com/environment/060815_gw_hurricanes.html&lt;/a&gt; &lt;span style=""&gt; &lt;/span&gt;&lt;span style="color:red;"&gt;What was hurricane activity like 200 years ago?&lt;/span&gt; &lt;/p&gt;   &lt;p&gt;&lt;span style=""&gt;            &lt;/span&gt;&lt;span style="color:red;"&gt;&lt;br /&gt;Is there something else contributing to the more frequent and violent hurricanes? &lt;/span&gt;Because of the seasonal changes in the ice, snow, atmospheric distribution, and perhaps because of movements in the material within the earth, the geographic poles constantly change position in relation to the earth’s surface - &lt;st1:city&gt;&lt;st1:place&gt;Chandler&lt;/st1:place&gt;&lt;/st1:city&gt; wobble. Scientists have resolved the change into two almost circular components, the first with a radius of about 6 meters and a period of 12 months, the second with a radius of 3-15 meters and a period of about 14 months.&lt;/p&gt;   &lt;p&gt;&lt;span style=""&gt;            &lt;/span&gt;&lt;br /&gt;The sun and moon, because of their varying distances and directions in relation to the earth, constantly vary their gravitational attractions on the earth. This makes the poles wander irregularly by about + or - 9 arc seconds from its average, or mean, position. This phenomenon is known as nutation and has a period of about 18.6 years. &lt;a href="http://library.thinkquest.org/29033/begin/earthsunmoon.htm"&gt;http://library.thinkquest.org/29033/begin/earthsunmoon.htm&lt;/a&gt; &lt;/p&gt;   &lt;p class="MsoNormal"&gt;&lt;span style=""&gt;            &lt;/span&gt;&lt;br /&gt;Records indicate a rising in sea surface temperature. Melting of polar ice and land-based glaciers is expected to contribute to the one half foot to three-feet sea level rise projected. &lt;a href="http://www.ucsusa.org/"&gt;http://www.ucsusa.org/&lt;/a&gt;&lt;span style=""&gt;  &lt;/span&gt;With the melting of polar ice, sea animals have changed their eating habits due to lack of usual food source and it has been mentioned that the &lt;st1:place&gt;&lt;st1:state&gt;Florida&lt;/st1:state&gt;&lt;/st1:place&gt; peninsula and costal regions could disappear.&lt;/p&gt;     &lt;p class="MsoNormal"&gt;&lt;span style="color:red;"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;span style=""&gt;          &lt;/span&gt;&lt;br /&gt;Problem - Will global warming keep progressing at an accelerated rate?&lt;span style=""&gt;  &lt;/span&gt;Will the earth get eventually to hot for life? How can humans stop the speed of global warming? Studies show that over next 100 years, the climate will increase (I have read different degrees). &lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt;     &lt;p class="MsoNormal"&gt;&lt;o:p&gt; &lt;/o:p&gt;&lt;span style=""&gt;            &lt;/span&gt;&lt;br /&gt;Health, agriculture, water resources, forests, wildlife and coastal areas are vulnerable to warming temperatures. Also with the melting of polar ice, it has been mentioned that the &lt;st1:place&gt;&lt;st1:state&gt;Florida&lt;/st1:state&gt;&lt;/st1:place&gt; peninsula and costal regions could disappear. With raising temperatures, heat related illness and more deaths occur as noted by newscasts and news articles. I know in our cities, temperatures are several degrees hotter than outside the area in the open plains. Being in &lt;st1:place&gt;&lt;st1:city&gt;Las Vegas&lt;/st1:city&gt;&lt;/st1:place&gt; this summer taught me this lesson, temperatures rose to near 120 degrees. &lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-6918559100572405875?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/6918559100572405875/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=6918559100572405875&amp;isPopup=true' title='5 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6918559100572405875'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6918559100572405875'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/cycle-teacher-as-researcher-js.html' title='Cycle A - Teacher as Researcher - JS'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>5</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-527771525928927367</id><published>2007-09-19T17:24:00.000-07:00</published><updated>2007-09-19T17:36:13.875-07:00</updated><title type='text'>Cycle A - Teacher as Researcher - JW</title><content type='html'>&lt;p class="MsoNormal"&gt;This is a subject that has perplexed me for quite some time now.&lt;span style=""&gt;  &lt;/span&gt;As I was going through grade school and high school we were taught that global warming was occurring because of our human actions on the earth and the high level of carbon dioxide that was being released into the atmosphere.&lt;span style=""&gt;  &lt;/span&gt;The message at that time was one of panic, “If we don’t do something quickly, our earth will be destroyed.”&lt;span style=""&gt;  &lt;/span&gt;Then as I attended college, the panic seemed to die down.&lt;span style=""&gt;  &lt;/span&gt;The media began to inform the public, that perhaps global warming was just a cycling of the earth’s temperature and didn’t have as much to do with humans as was previously thought.&lt;span style=""&gt;  &lt;/span&gt;This seemed to place society at ease and instead of being proactive about the problem, society became content to ignore it.&lt;span style=""&gt;  &lt;/span&gt;Now, in the past few years, we are once again getting conflicting information.&lt;span style=""&gt;  &lt;/span&gt;The media has swung back to their original conclusion that global warming is human caused.&lt;span style=""&gt;  &lt;/span&gt;Quite frankly, this has left me confused. I was interested in taking this class so that I could actually analyze some of the data myself.&lt;span style=""&gt;  &lt;/span&gt;I recently watched the Discovery Channel series, “Planet Earth”.&lt;span style=""&gt;  &lt;/span&gt;In the last segment of the series there were several scientists discussing the impact global warming is having on our earth, especially in the polar regions.&lt;span style=""&gt;  &lt;/span&gt;I have read several newspaper and magazine articles on the subject that covered this topic.&lt;span style=""&gt;  &lt;/span&gt;As of now, I have heard various claims supporting both sides of the debate, but have yet to see some data to back them up. &lt;span style=""&gt; &lt;/span&gt;I myself believe that humans have had an impact on global warming; to what degree I am not sure. &lt;span style=""&gt; &lt;/span&gt;I am looking forward to doing some data analysis and learning more on this subject from an objective viewpoint and not just from reading the media’s subjective opinions.&lt;span style=""&gt;  &lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-527771525928927367?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/527771525928927367/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=527771525928927367&amp;isPopup=true' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/527771525928927367'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/527771525928927367'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/cycle-teacher-as-researcher-jw.html' title='Cycle A - Teacher as Researcher - JW'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-2739543227278528731</id><published>2007-09-19T17:19:00.000-07:00</published><updated>2007-09-19T17:35:57.985-07:00</updated><title type='text'>Cycle A - Teacher as Researcher - CSA</title><content type='html'>&lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;What do I know about global warming?&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;Not much.&lt;span style=""&gt;  &lt;/span&gt;I mean, I’m a ScienceBlogs addict, I’ve seen “An Inconvenient Truth,” and I’ve read Chris Mooney’s “Storm World,” but I still don’t feel that I know the issues in any depth.&lt;/span&gt;&lt;/p&gt;         &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;The issues, as I see them, are inter-related – a change in one issue will ripple out to affect all of the others, much like a tug on one part of a spiderweb will distort the rest of the web – and perhaps tear it beyond functionality.&lt;o:p&gt;&lt;/o:p&gt;&lt;/span&gt;&lt;/p&gt; &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;First, how do we know that global warming is occurring?&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;Second, how do we know that the warming is exacerbated by human activity?&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;Third, given #1 &amp;amp; #2, how can we as science teachers/communicators serve as trusted, reliable sources of information for the general public?&lt;span style=""&gt;  &lt;/span&gt;&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;It’s my understanding that we know global warming is occurring through multiple areas of study.&lt;span style=""&gt;  &lt;/span&gt;Ice cores from &lt;st1:city&gt;&lt;st1:place&gt;Vladivostok&lt;/st1:place&gt;&lt;/st1:city&gt; in the Antarctic have tiny pockets of air that were encapsulated over thousands and thousands of years.&lt;span style=""&gt;  &lt;/span&gt;Some ratio of isotopes found within those air pockets can indicate the air temperature at the time the snow was compacted into glacial ice.&lt;span style=""&gt;  &lt;/span&gt;Other than that, I don’t remember what particular evidence there is for global warming.&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;&lt;span style="font-style: italic;"&gt;(Which brings me to a pet peeve . . . in one of our readings – sorry, don’t remember which – the early Earth atmosphere was described in great detail.&lt;/span&gt;&lt;span style="font-style: italic;"&gt;  &lt;/span&gt;&lt;span style="font-style: italic;"&gt;That’s the good news.&lt;/span&gt;&lt;span style="font-style: italic;"&gt;  &lt;/span&gt;&lt;span style="font-style: italic;"&gt;The bad news is that there is *no* description to indicate *how* these details are known!&lt;/span&gt;&lt;span style="font-style: italic;"&gt;  &lt;/span&gt;&lt;span style="font-style: italic;"&gt;If we’re to teach science as a process, why isn’t this information also included?)&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;It’s easy to see on the small scale how human activity undoubtedly influences the environment.&lt;span style=""&gt;  &lt;/span&gt;But given the vastness of the oceans, and the towering summer thunderheads which seem to represent an atmosphere of incredible height, it’s more difficult for us relatively puny humans to visualize having any impact on the global environment.&lt;span style=""&gt;  &lt;/span&gt;The “hockey stick” and CO2/temperature v. time graphs in the movie “An Inconvenient Truth” were explicit in their linkage of human activity to temperature change.&lt;span style=""&gt;  &lt;/span&gt;&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;But global warming deniers have their audiences, too.&lt;span style=""&gt;  &lt;/span&gt;Critics are quick to point out that in the 1970s, global cooling was our great fear.&lt;span style=""&gt;  &lt;/span&gt;Last spring, a well-educated, open-minded FHSU faculty member sent me an email with a link to an ostensible global warming quiz.&lt;span style=""&gt;  &lt;/span&gt;One catch – the quiz was decidedly at odds with accepted science, and was amateurishly, non-objectively written.&lt;span style=""&gt;  &lt;/span&gt;Googling produced the fact that the ‘quiz’ writer is a well-known activist who works for the state of &lt;st1:state&gt;&lt;st1:place&gt;West   Virginia&lt;/st1:place&gt;&lt;/st1:state&gt; (I think . . . ) to help promote their coal mines.&lt;span style=""&gt;  &lt;/span&gt;&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;So it looks like much of our job must focus on figuring out which sources of information are reliable, and which are suspect – which brings us to the last point.&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;We all labor under the “those who can’t, teach” misconception of ineptitude on our part.&lt;span style=""&gt;  &lt;/span&gt;How can we convince our students – and by extension, their parents and our community – that we are a valuable scientific resource?&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;As science teachers, we have unique gifts:&lt;span style=""&gt;  &lt;/span&gt;we are trained communicators with strong science backgrounds.&lt;span style=""&gt;  &lt;/span&gt;As such, we should be outspoken within our communities in our support of accepted, mainstream science.&lt;span style=""&gt;  &lt;/span&gt;But . . . as I mentioned before, we have *very* little credibility in the eyes of the public.&lt;span style=""&gt;  &lt;/span&gt;I don’t have the first clue how to fix that situation, and I’d like to learn.&lt;span style=""&gt;  &lt;/span&gt;Chris Mooney &amp;amp; Matthew Nisbet have addressed the issue of “framing” at their ScienceBlog, &lt;a href="http://scienceblogs.com/intersection"&gt;http://scienceblogs.com/intersection&lt;/a&gt;.&lt;span style=""&gt;  &lt;/span&gt;By “framing,” we are called to know our science so well that we are able to relate science issues to our fellow community members in a manner that is accurate yet understandable.&lt;span style=""&gt;  &lt;/span&gt;Needless to say, this issue has aroused great controversy, as some in the scientific community see this as “dumbing down” science.&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;However . . . think about sex.&lt;span style=""&gt;  &lt;/span&gt;[Not in &lt;span style="font-style: italic;"&gt;that&lt;/span&gt; way . . . ]&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;Think about explaining it to your kids!&lt;span style=""&gt;  &lt;/span&gt;Describing “where babies come from” to a 5-year-old is much different than discussing the more complex issues with teenagers.&lt;span style=""&gt;  &lt;/span&gt;It’s not that the 5-year-old is being given “bad” information – just that which is appropriate for her background knowledge.&lt;span style=""&gt;  &lt;/span&gt;&lt;/span&gt;&lt;/p&gt;     &lt;p  class="MsoNormal" style="font-family:verdana;"&gt;&lt;span style="font-size:85%;"&gt;&lt;o:p&gt;&lt;/o:p&gt;&lt;br /&gt;It’s the same with science issues.&lt;span style=""&gt;  &lt;/span&gt;We have to figure out how to express ourselves succinctly yet accurately when it comes to the science of global warming and human-related causes.&lt;/span&gt;&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-2739543227278528731?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/2739543227278528731/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=2739543227278528731&amp;isPopup=true' title='3 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/2739543227278528731'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/2739543227278528731'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/cycle-teacher-as-researcher-csa.html' title='Cycle A - Teacher as Researcher - CSA'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>3</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-6721196776340728818</id><published>2007-09-19T17:17:00.000-07:00</published><updated>2007-09-19T17:34:43.548-07:00</updated><title type='text'>Cycle A - Teacher as Researcher - JTW</title><content type='html'>&lt;p  style="margin: 0in 0in 10pt; font-family: georgia;font-family:arial;"&gt;&lt;span style="font-size:85%;"&gt;I believe “Global Warming” is a kitchy catch phrase for a real event that is occurring as we speak.&lt;span&gt;  &lt;/span&gt;I have watched “An Inconvenient Truth” which provides evidence from many scientists that the rapid rise in CO&lt;sub&gt;2&lt;/sub&gt; levels is a trend that, if it continues at the current rate, will trap enough solar energy to cause—for one thing--serious depletion of the polar ice caps, which causes a domino effect of change within the Earth System.&lt;span&gt;  &lt;/span&gt;While the movie purports that humanity is the cause of the unprecedented speed with which this is occurring, other scientist and nay-sayers still claim the cycle is natural, if one were to look at Earth’s history of climatic ups and downs.&lt;span&gt;  &lt;/span&gt;They say the evidence is exaggerated.&lt;span&gt;  &lt;/span&gt;&lt;strong&gt;&lt;i&gt;I&lt;/i&gt;&lt;/strong&gt; believe that it is OBVIOUS that humanity has changed this world more abruptly than any other species, and quite possibly any other &lt;i&gt;event &lt;/i&gt;in Earth’s history, save perhaps theoretical asteroid collisions blamed for mass extinctions in the past.&lt;span&gt;  &lt;/span&gt;&lt;/span&gt;&lt;/p&gt; &lt;p  style="margin: 0in 0in 10pt; font-family: georgia;font-family:arial;"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;Aside from the debate on whether or not we are causing rapid global warming, there is PROOF we have caused changes to the planet in many other ways.&lt;span&gt;  &lt;/span&gt;We have damaged the oceans with our human behaviors, killing life-sustaining reefs, according to the World Resources Institute (who studied human affects on the reefs near Belize) and the &lt;span style="color: rgb(51, 51, 51);"&gt;Coral Reef Monitoring Network (see &lt;/span&gt;&lt;a href="http://www.livescience.com/environment/coral_reef_041207.html"&gt;http://www.livescience.com/environment/coral_reef_041207.html&lt;/a&gt;&lt;span style="color: rgb(51, 51, 51);"&gt;).&lt;span&gt;  &lt;/span&gt;We have polluted the waters of this planet, possibly beyond repair, with industrial chemicals, human waste, and other pathogens (including artificial hormones and unused medicines [see &lt;/span&gt;&lt;a href="http://www.bu.edu/sjmag/scimag2005/features/drugsinwater.htm"&gt;http://www.bu.edu/sjmag/scimag2005/features/drugsinwater.htm&lt;/a&gt;&lt;span style="color: rgb(51, 51, 51);"&gt;]) we mindlessly dump into the waters (point-pollution evidence is irrefutable in this argument).&lt;span&gt;  &lt;/span&gt;While the EPA and NOAA may monitor changes in our own nation’s fresh water supply, other countries, like China and India, are dumping more and more toxins into the system with seriously lax regulations and enforcements (according to a recent report, the &lt;/span&gt;&lt;/span&gt;&lt;span style="font-size:85%;"&gt;&lt;span style="line-height: 115%;"&gt;deputy minister of construction in China says that &lt;/span&gt;90 percent of China's cities and 75 percent of its lakes have some degree of damaged water [see &lt;a href="http://www.chinadaily.com.cn/english/doc/2005-06/07/content_449451.htm"&gt;http://www.chinadaily.com.cn/english/doc/2005-06/07/content_449451.htm&lt;/a&gt;]).&lt;span style="line-height: 115%;"&gt; We have raped the rainforests through clear-cutting and have drained the wetlands to make room for farm ground and cities.&lt;span&gt;  &lt;/span&gt;We have helped in the rapid transport of damaging invasive species all around the world—by plane, car, and boat (see &lt;/span&gt;&lt;a href="http://www.ucsusa.org/invasive_species/invasive-species-update.html"&gt;&lt;span style="line-height: 115%;"&gt;http://www.ucsusa.org/invasive_species/invasive-species-update.html&lt;/span&gt;&lt;/a&gt;&lt;/span&gt;&lt;span style="font-size:85%;"&gt;&lt;span style="line-height: 115%;"&gt;).&lt;span&gt;  &lt;/span&gt;We have putrefied the air in our cities with our wasteful consumption of petroleum products and disregard for the impact it places on the environment.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt; &lt;span style="font-family: georgia;font-family:arial;font-size:85%;"  &gt;&lt;span style="line-height: 115%;"&gt;&lt;br /&gt;How is it, then, that we can &lt;i&gt;believe&lt;/i&gt; we are not causing damage to this planet?&lt;span&gt;  &lt;/span&gt;Look at all we do, in the name of “Human as Superior Being.”&lt;span&gt;  &lt;/span&gt;How can human beings continue to behave this way without guilt?&lt;span&gt;  &lt;/span&gt;What can we do to stop this human invasion of the planet?&lt;span&gt;  &lt;/span&gt;I know this might all sound too philosophical for a science class, but I wonder what it is going to take to WAKE US UP!&lt;span&gt;  &lt;/span&gt;Is money the driving factor to all this behavior (I think I already know the answer to that one)?&lt;/span&gt;&lt;/span&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-6721196776340728818?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/6721196776340728818/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=6721196776340728818&amp;isPopup=true' title='2 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6721196776340728818'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/6721196776340728818'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/cycle-teacher-as-researcher-jtw.html' title='Cycle A - Teacher as Researcher - JTW'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>2</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-262288387495345392</id><published>2007-09-19T05:14:00.000-07:00</published><updated>2007-09-19T05:46:18.873-07:00</updated><title type='text'>ESSEA Cycle 2 - Team Tasks</title><content type='html'>&lt;p&gt;&lt;b&gt;Here are the group investigation steps:&lt;/b&gt;&lt;/p&gt; &lt;ul&gt;&lt;li&gt; identify the topic or problem,&lt;/li&gt;&lt;ul&gt;&lt;li&gt;&lt;span style="font-style: italic;"&gt;We've done this, right? - global warming is our topic?&lt;/span&gt;&lt;br /&gt;&lt;/li&gt;&lt;/ul&gt;&lt;li&gt; decide what we need to conduct the study and ask appropriate questions,&lt;/li&gt;&lt;li&gt; gather and analyze information,&lt;/li&gt;&lt;li&gt; and prepare a report or other evidence of finishing the investigation.  &lt;/li&gt;&lt;/ul&gt;&lt;p&gt;&lt;b&gt;What we need to do:&lt;br /&gt;&lt;/b&gt;&lt;/p&gt;  &lt;ul&gt;&lt;li&gt;Post our questions in the discussion space in the Teacher as Researcher Discussion Space.&lt;/li&gt;&lt;ul&gt;&lt;li&gt;&lt;span style="font-style: italic;"&gt;Well, we can use this venue, if it will help; if it just gets in the way, fuggedaboudit.&lt;/span&gt;&lt;br /&gt;&lt;/li&gt;&lt;/ul&gt;&lt;li&gt;Review our teammates' questions. &lt;/li&gt;&lt;li&gt;List the key questions and plan how to investigate them as a team.&lt;/li&gt;&lt;li&gt;List answers to our questions as we build knowledge together.&lt;/li&gt;&lt;/ul&gt;        &lt;b&gt;Deadline: &lt;/b&gt; Friday, September 21 2007 11:59 PM (Central Time)&lt;br /&gt;&lt;div style="text-align: center;"&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://regmedia.co.uk/2007/06/27/usb_panic_1.png"&gt;&lt;img style="cursor: pointer; width: 159px; height: 190px;" src="http://regmedia.co.uk/2007/06/27/usb_panic_1.png" alt="" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-262288387495345392?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/262288387495345392/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=262288387495345392&amp;isPopup=true' title='5 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/262288387495345392'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/262288387495345392'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/essea-cycle-2-team-tasks.html' title='ESSEA Cycle 2 - Team Tasks'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>5</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-3814457669617791183</id><published>2007-09-19T04:21:00.000-07:00</published><updated>2007-09-19T05:12:42.974-07:00</updated><title type='text'>ESSEA Cycle 2</title><content type='html'>[looking in the direction of Blackboard at FHSU - &lt;span style="font-style: italic;"&gt;scutta mal occhio, pu pu pu&lt;/span&gt;!]&lt;br /&gt;&lt;br /&gt;We have some tasks to accomplish by this Friday.  I'll get them listed here, and we can discuss them in the comments.  To comment, just click on the &lt;span style="font-style: italic;"&gt;Comments&lt;/span&gt; link at the bottom of this post.&lt;br /&gt;&lt;br /&gt;We'll get through this, ladies!&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-3814457669617791183?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/3814457669617791183/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=3814457669617791183&amp;isPopup=true' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/3814457669617791183'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/3814457669617791183'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/09/essea-cycle-2.html' title='ESSEA Cycle 2'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-3326062467251335024</id><published>2007-07-14T15:51:00.000-07:00</published><updated>2007-07-14T15:53:48.124-07:00</updated><title type='text'>"Why Does the Sun Shine?"</title><content type='html'>Had a request to post the &lt;a href="http://www.niehs.nih.gov/kids/lyrics/whysunshine.htm"&gt;lyrics&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;&lt;quote&gt;   &lt;br /&gt;The sun is a mass of incandescent gas&lt;br /&gt;A gigantic nuclear furnace&lt;br /&gt;Where Hydrogen is built into Helium&lt;br /&gt;At a temperature of millions of degrees&lt;br /&gt;&lt;br /&gt;The sun is hot, the sun is not&lt;br /&gt;A place where we could live&lt;br /&gt;But here on Earth there'd be no life&lt;br /&gt;Without the light it gives&lt;br /&gt;&lt;br /&gt;We need its light, we need its heat&lt;br /&gt;The sun light that we seek&lt;br /&gt;The sun light comes from our own sun's&lt;br /&gt;Atomic energy&lt;br /&gt;&lt;br /&gt;The sun is a mass of incandescent gas&lt;br /&gt;A gigantic nuclear furnace&lt;br /&gt;Where Hydrogen is built into Helium&lt;br /&gt;At a temperature of millions of degrees&lt;br /&gt;&lt;br /&gt;The sun is hot...&lt;br /&gt;&lt;br /&gt;The sun is so hot that everything on it is a gas&lt;br /&gt;Aluminum, Copper, Iron, and many others&lt;br /&gt;&lt;br /&gt;The sun is large...&lt;br /&gt;&lt;br /&gt;If the sun were hollow, a million Earth's would fit inside&lt;br /&gt;And yet, it is only a middle size star&lt;br /&gt;&lt;br /&gt;The sun is far away...&lt;br /&gt;&lt;br /&gt;About 93,000,000 miles away&lt;br /&gt;And that's why it looks so small&lt;br /&gt;&lt;br /&gt;But even when it's out of sight&lt;br /&gt;The sun shines night and day&lt;br /&gt;&lt;br /&gt;We need its heat, we need its light&lt;br /&gt;The sun light that we seek&lt;br /&gt;The sun light comes from our own sun's&lt;br /&gt;Atomic energy&lt;br /&gt;&lt;br /&gt;Scientists have found that the sun is a huge atom smashing machine&lt;br /&gt;The heat and light of the sun are caused by nuclear reactions between&lt;br /&gt;Hydrogen, Nitrogen, Carbon, and Helium&lt;br /&gt;&lt;br /&gt;The sun is a mass of incandescent gas&lt;br /&gt;A gigantic nuclear furnace&lt;br /&gt;Where Hydrogen is built into Helium&lt;br /&gt;At a temperature of millions of degrees&lt;/quote&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-3326062467251335024?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/3326062467251335024/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=3326062467251335024&amp;isPopup=true' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/3326062467251335024'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/3326062467251335024'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/07/why-does-sun-shine.html' title='&quot;Why Does the Sun Shine?&quot;'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-2482048114831863257</id><published>2007-07-11T13:20:00.001-07:00</published><updated>2007-07-11T13:24:47.605-07:00</updated><title type='text'>Virtual Earthquake</title><content type='html'>For schools with easy access to computer labs or with 1-1 laptop initiatives, try this &lt;a href="http://www.sciencecourseware.org/eec/Earthquake"&gt;"Virtual Earthquake"&lt;/a&gt; activity.  Students measure s-p lag times, estimate the energy of the earthquake using a nomogram, 'draw' the circles for triangulation, and practice using longitude &amp; latitude measurements.&lt;br /&gt;&lt;br /&gt;Enjoy!&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-2482048114831863257?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/2482048114831863257/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=2482048114831863257&amp;isPopup=true' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/2482048114831863257'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/2482048114831863257'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/07/virtual-earthquake.html' title='Virtual Earthquake'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-4074152641526693101.post-5896463347141234248</id><published>2007-07-11T07:43:00.000-07:00</published><updated>2007-07-11T07:49:04.139-07:00</updated><title type='text'>What's the point?</title><content type='html'>As if we all need one more thing to do, right?&lt;br /&gt;&lt;br /&gt;But we're going pretty fast, and a lot of teaching ideas are being described with no time to record them for posterity.&lt;br /&gt;&lt;br /&gt;Here's a spot for you to - pretty please! - summarize your idea so the rest of us can use it.  You can do so by making your own post (get your email to me so I can add you as an author here) or in the comments section of any post.  I'll organize this on a day-by-day basis.&lt;br /&gt;&lt;br /&gt;It's normal to be thinking "but my ideas aren't that great!"  Oh, yes they are!  Sure, it takes guts to share, but that's how we'll all improve.&lt;br /&gt;&lt;br /&gt;Here we go!&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/4074152641526693101-5896463347141234248?l=earthmodeling.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://earthmodeling.blogspot.com/feeds/5896463347141234248/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=4074152641526693101&amp;postID=5896463347141234248&amp;isPopup=true' title='8 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/5896463347141234248'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/4074152641526693101/posts/default/5896463347141234248'/><link rel='alternate' type='text/html' href='http://earthmodeling.blogspot.com/2007/07/whats-point.html' title='What&apos;s the point?'/><author><name>Cheryl Shepherd-Adams</name><uri>http://www.blogger.com/profile/06324183099292364031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='32' src='http://www.physics.sfsu.edu/~lea/courses/grad/rotatingsun.gif'/></author><thr:total>8</thr:total></entry></feed>
